Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005
Understanding the amount and timing of stream inflow to Linnevatnet is of critical importance when attempting to quantify sedimentation. Linnebreen, located 6km south of Linnevatnet, is the largest source for inflow to Linnevatnet. Mass balance measurements, via traditional stake methods, provide a...
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Arctic Data Center
2013
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Online Access: | https://doi.org/10.18739/A2M90226G |
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dataone:doi:10.18739/A2M90226G |
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openpolar |
institution |
Open Polar |
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Arctic Data Center (via DataONE) |
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dataone:urn:node:ARCTIC |
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EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS MANNED FIELD STATION HOURLY TO DAILY DAILY TO WEEKLY ANNUAL 1 MINUTE TO 1 HOUR MONTHLY TO ANNUAL WEEKLY TO MONTHLY inlandWaters oceans environment climatologyMeteorologyAtmosphere |
spellingShingle |
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS MANNED FIELD STATION HOURLY TO DAILY DAILY TO WEEKLY ANNUAL 1 MINUTE TO 1 HOUR MONTHLY TO ANNUAL WEEKLY TO MONTHLY inlandWaters oceans environment climatologyMeteorologyAtmosphere Caleb Schiff Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 |
topic_facet |
EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS MANNED FIELD STATION HOURLY TO DAILY DAILY TO WEEKLY ANNUAL 1 MINUTE TO 1 HOUR MONTHLY TO ANNUAL WEEKLY TO MONTHLY inlandWaters oceans environment climatologyMeteorologyAtmosphere |
description |
Understanding the amount and timing of stream inflow to Linnevatnet is of critical importance when attempting to quantify sedimentation. Linnebreen, located 6km south of Linnevatnet, is the largest source for inflow to Linnevatnet. Mass balance measurements, via traditional stake methods, provide a tool to quantify Linnebreen’s contribution. Furthermore, mass balance studies shed light on the larger climatic regime of the area during the year of observation and provide a means to determine the “health” of the glacier. Historical records of Linnebreen’s 20th century retreat are preserved in aerial photos. Analysis of photos can give insight into the rate of retreat, providing context for the assessment of Linnebreen’s “health.” As anthropogenic climate change becomes a topic of increasing scientific discussion, especially in the arctic, monitoring such ice masses acquires further significance. This study asks the following questions: What is the current “health” of Linnebreen? How has the beginning of the 21st century compared to the past 100 years? What and when does Linnebreen melt during the summer? What is the main agent of melting? |
format |
Dataset |
author |
Caleb Schiff |
author_facet |
Caleb Schiff |
author_sort |
Caleb Schiff |
title |
Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 |
title_short |
Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 |
title_full |
Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 |
title_fullStr |
Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 |
title_full_unstemmed |
Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 |
title_sort |
unsustainable glacier ablation at 78° n latitude, linnébreen, svalbard, 2005 |
publisher |
Arctic Data Center |
publishDate |
2013 |
url |
https://doi.org/10.18739/A2M90226G |
op_coverage |
ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > SVALBARD AND JAN MAYEN ENVELOPE(11.64,14.104,78.081,77.943) |
long_lat |
ENVELOPE(20.000,20.000,78.000,78.000) ENVELOPE(13.933,13.933,77.967,77.967) ENVELOPE(11.64,14.104,78.081,77.943) |
geographic |
Arctic Svalbard Jan Mayen Svalbard Linnébreen |
geographic_facet |
Arctic Svalbard Jan Mayen Svalbard Linnébreen |
genre |
Arctic Climate change glacier Ice Sheet Jan Mayen North Atlantic Svalbard |
genre_facet |
Arctic Climate change glacier Ice Sheet Jan Mayen North Atlantic Svalbard |
op_doi |
https://doi.org/10.18739/A2M90226G |
_version_ |
1800870081068007424 |
spelling |
dataone:doi:10.18739/A2M90226G 2024-06-03T18:46:42+00:00 Unsustainable Glacier Ablation at 78° N latitude, Linnébreen, Svalbard, 2005 Caleb Schiff ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > SVALBARD AND JAN MAYEN ENVELOPE(11.64,14.104,78.081,77.943) 2013-11-10T00:00:00Z https://doi.org/10.18739/A2M90226G unknown Arctic Data Center EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTS EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > LAKE LEVELS EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > VARVE DEPOSITS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > DEGRADATION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIER MASS BALANCE/ICE SHEET MASS BALANCE EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > SEDIMENT TRANSPORT EARTH SCIENCE > OCEANS > MARINE SEDIMENTS > TURBIDITY EARTH SCIENCE > LAND SURFACE > LAND TEMPERATURE > LAND SURFACE TEMPERATURE EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > ENTRAINMENT EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > SOIL TEMPERATURE EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERIGLACIAL PROCESSES EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SUSPENDED SOLIDS IN SITU/LABORATORY INSTRUMENTS > SAMPLERS > GRABBERS/TRAPS/COLLECTORS > SEDIMENT TRAPS IN SITU/LABORATORY INSTRUMENTS > CORERS > SEDIMENT CORERS IN SITU/LABORATORY INSTRUMENTS > CONDUCTIVITY SENSORS > CONDUCTIVITY METERS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PHOTON/OPTICAL DETECTORS > CAMERAS > CAMERAS EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > PROFILERS/SOUNDERS > TEMPERATURE PROFILERS IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS IN SITU/LABORATORY INSTRUMENTS > GAUGES > STREAM GAUGES EARTH REMOTE SENSING INSTRUMENTS > PASSIVE REMOTE SENSING > POSITIONING/NAVIGATION > GPS > GPS > GLOBAL POSITIONING SYSTEM EARTH REMOTE SENSING INSTRUMENTS > ACTIVE REMOTE SENSING > PROFILERS/SOUNDERS > ACOUSTIC SOUNDERS > ECHO SOUNDERS IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES IN SITU/LABORATORY INSTRUMENTS > CORERS > CORING DEVICES IN SITU/LABORATORY INSTRUMENTS > PROBES > STEEL MEASURING TAPE IN SITU/LABORATORY INSTRUMENTS > CURRENT/WIND METERS > CURRENT METERS MANNED FIELD STATION HOURLY TO DAILY DAILY TO WEEKLY ANNUAL 1 MINUTE TO 1 HOUR MONTHLY TO ANNUAL WEEKLY TO MONTHLY inlandWaters oceans environment climatologyMeteorologyAtmosphere Dataset 2013 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2M90226G 2024-06-03T18:11:09Z Understanding the amount and timing of stream inflow to Linnevatnet is of critical importance when attempting to quantify sedimentation. Linnebreen, located 6km south of Linnevatnet, is the largest source for inflow to Linnevatnet. Mass balance measurements, via traditional stake methods, provide a tool to quantify Linnebreen’s contribution. Furthermore, mass balance studies shed light on the larger climatic regime of the area during the year of observation and provide a means to determine the “health” of the glacier. Historical records of Linnebreen’s 20th century retreat are preserved in aerial photos. Analysis of photos can give insight into the rate of retreat, providing context for the assessment of Linnebreen’s “health.” As anthropogenic climate change becomes a topic of increasing scientific discussion, especially in the arctic, monitoring such ice masses acquires further significance. This study asks the following questions: What is the current “health” of Linnebreen? How has the beginning of the 21st century compared to the past 100 years? What and when does Linnebreen melt during the summer? What is the main agent of melting? Dataset Arctic Climate change glacier Ice Sheet Jan Mayen North Atlantic Svalbard Arctic Data Center (via DataONE) Arctic Svalbard Jan Mayen Svalbard ENVELOPE(20.000,20.000,78.000,78.000) Linnébreen ENVELOPE(13.933,13.933,77.967,77.967) ENVELOPE(11.64,14.104,78.081,77.943) |